Tropospheric ozone is involved in a complex web of interactions with other atmospheric gases and particles, and through ecosystem interactions with the N-cycle and climate change. Ozone itself is a greenhouse gas, causing warming, and reductions in biomass and carbon sequestration
caused by ozone provide a further indirect warming effect. Ozone also has cooling effects, however, for example, through impacts on aerosols and diffuse radiation. Ecosystems are both a source of ozone precursors (especially of hydrocarbons, but also nitrogen oxides), and a sink through deposition processes. The interactions with vegetation, atmospheric chemistry and aerosols are complex, and only partially understood. Levels and patterns of global exposure to ozone may change dramatically over the next 50 years, impacting global warming, air quality, global food production and ecosystem function.

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BibTeX @article{Simpson2014,author={Simpson, David and Arneth, Almut and Mills, Gina and Solberg, Sverre and Uddling, Johan},title={Ozone - the persistent menace; interactions with the N cycle and climate change},journal={Current Opinion in Environmental Sustainability},issn={1877-3435},volume={9-10},pages={9-19},abstract={Tropospheric ozone is involved in a complex web of interactions with other atmospheric gases and particles, and through ecosystem interactions with the N-cycle and climate change. Ozone itself is a greenhouse gas, causing warming, and reductions in biomass and carbon sequestration
caused by ozone provide a further indirect warming effect. Ozone also has cooling effects, however, for example, through impacts on aerosols and diffuse radiation. Ecosystems are both a source of ozone precursors (especially of hydrocarbons, but also nitrogen oxides), and a sink through deposition processes. The interactions with vegetation, atmospheric chemistry and aerosols are complex, and only partially understood. Levels and patterns of global exposure to ozone may change dramatically over the next 50 years, impacting global warming, air quality, global food production and ecosystem function.},year={2014},keywords={Ozone, aerosol, forests, biomass, climate},}

RefWorks RT Journal ArticleSR ElectronicID 207889A1 Simpson, DavidA1 Arneth, AlmutA1 Mills, GinaA1 Solberg, SverreA1 Uddling, JohanT1 Ozone - the persistent menace; interactions with the N cycle and climate changeYR 2014JF Current Opinion in Environmental SustainabilitySN 1877-3435VO 9-10SP 9AB Tropospheric ozone is involved in a complex web of interactions with other atmospheric gases and particles, and through ecosystem interactions with the N-cycle and climate change. Ozone itself is a greenhouse gas, causing warming, and reductions in biomass and carbon sequestration
caused by ozone provide a further indirect warming effect. Ozone also has cooling effects, however, for example, through impacts on aerosols and diffuse radiation. Ecosystems are both a source of ozone precursors (especially of hydrocarbons, but also nitrogen oxides), and a sink through deposition processes. The interactions with vegetation, atmospheric chemistry and aerosols are complex, and only partially understood. Levels and patterns of global exposure to ozone may change dramatically over the next 50 years, impacting global warming, air quality, global food production and ecosystem function.LA engDO 10.1016/j.cosust.2014.07.008LK http://dx.doi.org/10.1016/j.cosust.2014.07.008LK http://publications.lib.chalmers.se/records/fulltext/207889/local_207889.pdfOL 30